Geological Terms Beginning With "G"
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A black, coarse-grained intrusive igneous rock that is the compositional equivalent of basalt. Composed of calcium-rich feldspars, pyroxene and possibly olivine, but containing little if any quartz.
A measured height of water above a reference datum. Frequently used to describe the height of water in a stream, lake, well, canal or other water body.
A facility on a stream, lake, canal, reservoir or other water body where instruments are installed to automatically monitor the water. Measurments such as stage, discharge, water temperature and pH are automatically taken and transmitted to hydrologists via satellite, radio or telephone. Measurements from these stations are useful for a wide variety of flood prediction, water management, recreation and navigation purposes.
Garnet is the name of a group of silicate minerals that share a common crystal structure but they vary in composition. Most garnets are red in color, but the mineral also occurs in orange, yellow, purple, green, pink, black, and other colors. Shown in the photo from top to bottom are: spessartine, almandine, mali, rhodolite and tsavorite. In addition to being used as a gem, garnet is used as an abrasive, filter medium, sand-blasting granule and waterjet cutting granule.
The geographic area that is directly above an underground accumulation of natural gas that is commercially viable.
A pipeline that carries natural gas between a production well and a main transmission line.
A network of small pipelines that connect producing wells to the main transmission system.
There is no universally agreed upon definition for the word "gemstone". The word usually triggers an image of attractive mineral materials that have been fashioned into gems to be worn for personal adornment. Some people believe that gemstones should also be durable, rare, valuable and skillfully cut - but some items formally called "gemstones" lack all of these. Many gemstones are rocks, organic materials, mineraloids or even objects from space that lack durability, rarity, intrinsic value and are used in their natural state. As an example consider a small pearl used in an inexpensive necklace sold at Walmart. Hundreds of materials have been used as gemstones, see photos of over 100 here.
A diagram that shows the vertical sequence of rock units present beneath a
given location with the oldest at the bottom and youngest at the top. They
are typically drawn to approximate scale with proportional rock unit
thicknesses. Colors and standardized symbols are usually added to
graphically communicate rock types and some of their more important
features. Geologic columns prepared for regions will have generalized
thicknesses and rock unit features that show relationships that change over
Geology is the study of the Earth, the materials of which it is made, the structure of those materials, and the processes acting upon them. It includes the study of organisms that have inhabited our planet. An important part of geology is the study of how Earth’s materials, structures, processes and organisms have changed over time.
The science of Earth's landforms, their description, classification, distribution, origin and significance.
The progressive increase of temperature with depth into the Earth. Often displayed graphically as a chart similar to the image at right which shows the geothermal gradient in the Carson Sink area of Nevada from a USGS report.
A hot spring that intermittently erupts a spray of steam and hot water. Caused by the heating of ground water within a confined opening in hot rock.
A very gradual uplift of Earth's crust that occurs after the weight of a thick continental ice sheet (which produced subsidence) has melted away.
Grooves and scratches on a bedrock surface that were produced by the movement of a glacier. The orientation of the striations gives evidence to the direction of glacial movement.
A valley with a U-shaped cross section that was cut by an alpine glacier.
A thick mass of ice that forms on land from an accumulation and recrystallization of snow significant enough to persist through the summer and grow year by year. There are two basic types of glaciers: 1) valley (or alpine) glaciers that creep downslope under the influence of gravity, and 2) continental glaciers that flow outward from a thick central area under their own weight.
An amorphous (without crystal structure) igneous rock that forms from very rapid cooling of magma. The rapid cooling does not provide enough time for crystal growth.
A coarse-grained, foliated rock produced by regional metamorphism. The mineral grains within gneiss are elongated due to pressure and the rock has a compositional banding due to chemical activity.
Fine particles of native gold that have been weathered out of their host rock. They can be flake, nugget or wire-shaped particles. They can be mined from a placer deposit or milled from the rock of a lode. Image © Gilles_Paire, iStockphoto.
A piece native gold that has been weathered out of its host rock. Nuggets are found in placer deposits downslope from a lode. They might be found in soils, stream sediments or beach sediments. Nuggets are often smoothed and rounded, which is evidence of transport. They sometimes still contain pieces of host rock. They are generally not pure gold, instead being 80% to 95% gold. Image © Goruppa, iStockphoto.
A broad, shallow pan made of metal or rigid plastic that is used to separate the lighter fraction of a sediment from heavier grains. A shovel of stream sediment or soil is placed in the pan, the rocks are picked out and clinging soil or sediment scraped off, then the pan and sediment are immersed in the stream and moved in a manner that allows lighter grains to be removed by the current or sloshed over the rim of the pan. Considerable practice is required but an experienced person can separate sand, silt and mud from particles of gold or heavy mineral that are so small that they can barely be seen. View a gold panning demonstration. View gold panning supplies in the Geology.com Store.
An elongated, downthrown block bounded by two steeply dipping normal faults. Produced in an area of crustal extension.
A rock layer that has a progressive change in particle size from top to bottom. Most common is a sequence with coarse grains at the bottom and fining upwards, which is typically caused by a declining current velocity within the depositional environment.
A coarse-grained, intrusive igneous rock composed primarily of light colored minerals such as quartz, orthoclase, sodium plagioclase and muscovite mica. Granite is thought to be one of the main components of continental crust.
Clastic sedimentary particles of any composition that are over 2 mm in diameter.
A geographic area where the gravitational attraction is significantly higher or significantly lower than normal.
A warming of the atmosphere caused by carbon dioxide and water vapor in the lower portions of the atmosphere capturing heat that is radiated from and reflected by Earth's surface.
A low-grade metamorphic rock that frequently contains green minerals such as chlorite, epidote and talc.
A blanket of till that is deposited during the retreat of a glacier.
Groundwater or Ground Water
Water that exists below the water table in the zone of saturation. Groundwater moves slowly in the same direction that the water table slopes.
The American Geosciences Institute's Glossary of Geology 5th Edition has an entry for "groundwater" but none for "ground water". The National Ground Water Association uses "ground water" in their name but their mission statement includes "enhance the skills and credibility of all groundwater professionals". Their reports use "groundwater" with great frequency. Another organization is "The Groundwater Foundation" and they use "groundwater" regularly in their published information. The United States Geological Survey and the United States Environmental Protection Agency uses "groundwater" and "ground water" inconsistently in their reports.
A few people have written to Geology.com to scold and argue about how this term is used on our website. We refer those inquiries to the previously listed organizations who have a significantly higher stake in how the term is used. When they decide how to use it we will edit every incidence of the term on our website to follow their lead!
Groundwater Recharge Area
A location where surface water or precipitation can infiltrate into the ground and replenish the water supply of an aquifer.
A seamount with a flat top.
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